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A term used to describe a sensor (or sensors), the associated transducer(s), and the data readout or recording device.

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An evaporation pan in which the evaporation is measured from water in a pan floating in a larger body of water.

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Of or pertaining to rain.

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A hydrometeor consisting of an aggregate of microscopic and more-or-less hygroscopic water droplets suspended in the atmosphere. It reduces visibility to a lesser extent than fog. The relative humidity of mist is often less than 95 percent.

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RMS

Root Mean Square. This notation is used frequently with error analysis. In that context, it is the square root of the arithmetic mean of the squares of the deviations of the individual calibration points from the theoretical or ideal response.

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Thermometer for measuring the temperature in the soil at different depths.

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Low

An area of low barometric pressure, with its attendant system of winds. Also called a depression or cyclone.

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Programmable Read-Only Memory. Read-only memory which can be programmed by the user using a special hardware programmer.

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A thermometer, invented by James Six in 1782, which simultaneously indicates the maximum and minimum temperatures attained during a given interval of time. A U-tube min/max thermometer

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A unit of pressure which directly expresses the force exerted by the atmosphere. Equal to 1000 dynes/cm2 or 100 pascals.

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variable audio-modulated radiosonde developed at the Bureau of Standards and used by the United States weather services.

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A spring which is designed to achieve a fixed spring constant over a wide temperature range. Usually, this involves an alloy with high nickel content such as Ni-Span C. It is common for these springs to be stress relieved at elevated temperature after for ...

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The atmospheric pressure computed using station elevation as the reference datum level. Station pressure is usually the base value from which sea level pressure and altimeter setting are determined.

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The general term for dry atmospheric suspensoids, including dust, haze, smoke. and sand. Compare to hydrometeor.

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The algebraic difference between the upper and lower limits of the measuring range of an instrument, i.e. a thermometer with a range of -35 to 50

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A measure, proposed by Angstrom, of the precipitation effectiveness of a region.

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The time required for an instrument to register a designated percentage (frequently 90%) of a step change in the variable being measured.

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Very small precipitation drops (diameters less than 0.5 mm) that appear to float with air currents while falling in an irregular path. Unlike fog droplets, drizzle falls to the ground.

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See mote.

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The amount of sky covered or concealed by clouds or obscuring phenomena. It is reported in tenths, so that 0.0 indicates a clear sky and 1.0 (or 10/10) indicates a completely covered sky. The following classifications are used in aviation weather observat ...

Category:Meteorology